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源自偏振激光雷达和摄影分析的产生日冕的卷云特性。

Corona-producing cirrus cloud properties derived from polarization lidar and photographic analyses.

作者信息

Sassen K

出版信息

Appl Opt. 1991 Aug 20;30(24):3421-8. doi: 10.1364/AO.30.003421.

Abstract

Polarization lidar data are used to demonstrate that clouds composed of hexagonal ice crystals can generate multiple-ringed colored coronas. Although relatively uncommon in our mid-latitude cirrus sample (derived from Project FIRE extended time observations), the coronas are associated with unusual cloud conditions that appear to be effective in generating the displays. Invariably, the cirrus cloud tops are located at or slightly above elevated tropopauses (12.7-km MSL average height) at temperatures between -60 degrees and -70 degrees C. The cloud top region also generates relatively strong laser backscattering and unusually high 0.5-0.7 linear depolarization ratios. Color photograph analysis of corona ring angles indicates crystals with mean diameters of from 12 to 30 microm. The cirrus cloud types were mainly subvisual to thin (i.e., bluish-colored) cirrostratus, but also included fibrous cirrus. Estimated cloud optical thicknesses at the 0.694-microm laser wavelength ranged from 0.001 to 0.2, where the upper limit reflects the effects of multiple scattering and/or unfavorable changes in particle characteristics in deep cirrus clouds.

摘要

偏振激光雷达数据被用于证明由六角形冰晶组成的云可以产生多环彩色光晕。尽管在我们的中纬度卷云样本(源自火灾项目延长时间观测)中相对不常见,但这些光晕与似乎能有效产生这种现象的异常云况有关。卷云云顶总是位于对流层顶高度(平均海平面高度12.7千米)或略高于此高度,温度在-60摄氏度至-70摄氏度之间。云顶区域还会产生相对较强的激光后向散射以及异常高的0.5 - 0.7线性偏振比。对光晕环角度的彩色照片分析表明,晶体的平均直径在12至30微米之间。卷云类型主要是亚可见到薄的(即浅蓝色)卷层云,但也包括纤维状卷云。在0.694微米激光波长下估计的云光学厚度范围为0.001至0.2,其中上限反映了深卷云中多次散射和/或粒子特性不利变化的影响。

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